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| Registros recuperados : 266 | |
| 121. |  | ALVES, R. B. de O.; SILVA, H. P. da; ARAUJO FILHO, J. C. de; DOMINGUES, M. A. de O.; ALBUQUERQUE, J. O. de. Use of Vegetation Cover Index (ICV) to identify susceptible areas to desertification process in the semiarid municipalities of Pernambuco, Brazil. International Journal of Advanced Engineering Research and Science, v. 7, n. 1, p. 53-63, Jan. 2020.| Biblioteca(s): Embrapa Solos. |
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| 122. | | BOULET, R.; FRITSCH, E.; FILIZOLA, H. F.; ARAUJO FILHO, J. C. de; LEPRUN, J. C.; BARRETO, F.; BALAN, E.; TESSIER, D. Iron bands, fragipans and duripans in the Northeastern plateaus of Brazil: properties and genesis. Canadian Journal of Soil Science, v. 78, p. 519-530, 1998.| Biblioteca(s): Embrapa Meio Ambiente. |
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| 123. | | BOULET, R.; FRITSCH, E.; FILIZOLA, H. F.; ARAUJO FILHO, J. C. de; LEPRUN, J. C.; BARRETTO, F.; BALAN, E.; TESSIER, D. Iron bands, fragipans and duripans in the Northeastern plateaus of Brazil: properties and genesis. Canadian Journal of Soil Science, v. 78, n. 3, p. 519-530, Aug. 1998.| Biblioteca(s): Embrapa Solos. |
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| 124. | | OLIVEIRA NETO, M. B.; PARAHYBA, R. da B. V.; SANTOS, J. C. P. dos; LEITE, A. P.; ARAÚJO FILHO, J. C. de; CORRÊA, R. M. Levantamento detalhado de solos em uma área de reassentamento de colonos na bacia do Tucano, BA. CONGRESSO BRASILEIRO DE CIÊNCIA DO SOLO, 31., 2007, Gramado. Resumo| Biblioteca(s): Embrapa Solos. |
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| 130. | | PARAHYBA, R. da B. V.; SILVA, F. H. B. B. da; ARAUJO FILHO, J. C. de; SILVA, F. B. R. e; MAIA, J. L. T. Diagnóstico ambiental do município de Mirandiba: destaque antecipado do projeto de zoneamento agroecológico do estado de Pernambuco. In: CONGRESSO BRASILEIRO DE CIÊNCIA DO SOLO, 27., 1999, Brasília, DF. Resumos [...]. Planaltina, DF: Embrapa Cerrados, 1999. 1 CD-ROM.| Biblioteca(s): Embrapa Solos. |
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| 134. | | VAZ, G. J.; SILVA NETO, L. de F. da; OLIVEIRA, S. R. de M.; BOTELHO, F. P.; ARAUJO FILHO, J. C. de. Development of an expert system for classification of Brazilian soil profiles. In: WORLD CONGRESS OF SOIL SCIENCE, 21., 2018, Rio de Janeiro. Soil science: beyond food and fuel: proceedings... Viçosa, MG: SBCS, 2018. v. 1, p. 56-57. WCSS 2018.| Biblioteca(s): Embrapa Solos. |
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| 135. | | VAZ, G. J.; SILVA NETO, L. de F. da; OLIVEIRA, S. R. de M.; BOTELHO, F. P.; ARAUJO FILHO, J. C. de. Development of an expert system for classification of Brazilian soil profiles. In: WORLD CONGRESS OF SOIL SCIENCE, 21., 2018, Rio de Janeiro. Soil science: beyond food and fuel: abstracts. Viçosa, MG: SBCS, 2018. Não paginado. WCSS 2018. Publicado também em: WORLD CONGRESS OF SOIL SCIENCE, 21., 2018, Rio de Janeiro. Soil science beyond food and fuel: proceedings. Viçosa, MG: Sociedade Brasileira de Ciência do Solo, 2019. v. I, p. 56-57. Editores: Leandro Souza...| Biblioteca(s): Embrapa Agricultura Digital. |
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| 136. | | LOPES, H. L.; ACCIOLY, L. J. de O.; SILVA, F. H. B. B. da; SOBRAL, M. do C. M.; ARAUJO FILHO, J. C. de; CANDEIAS, A. L. B. Espacialização da umidade do solo por meio da temperatura da superfície e índice de vegetação. Revista Brasileira de Engenharia Agrícola e Ambiental, v. 15, n. 9, p. 973-980, set. 2011.| Biblioteca(s): Embrapa Algodão; Embrapa Solos. |
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| 138. | | BOLFE, E. L.; BATISTELLA, M.; RONQUIM, C. C.; BRAGANTINI, C.; ARAUJO FILHO, J. C. de; MACIA, C. J.; SANTANA, A. A. de; NETTO, J. M. O Corredor de Nacala: recursos naturais para agricultura. In: BATISTELLA, M.; BOLFE, E. L. Paralelos corredor de Nacala. Campinas, SP: Embrapa Monitoramento por Satélite, 2010.| Biblioteca(s): Embrapa Solos. |
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| 140. | | BOULET, R.; FRITSCH, E.; FILIZOLA, H. F.; ARAUJO FILHO, J. C. de; SILVA, F. B. R.; LAMOTTE, M.; LEPRUN J. C. Fragipans et duripans des plateaux lottoraux du Nordeste brésilien: stades d'évolution. In:WORL CONGRESS OF SOIL SCIENCE, 16., 1998, Montpellier, France. Symposium...CIRAD: Montepellier, France, 1998, CD Rom Symposion 15, p. 1-7.| Biblioteca(s): Embrapa Meio Ambiente. |
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| Registros recuperados : 266 | |
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 | Acesso ao texto completo restrito à biblioteca da Embrapa Solos. Para informações adicionais entre em contato com cnps.biblioteca@embrapa.br. |
Registro Completo
|
Biblioteca(s): |
Embrapa Solos. |
|
Data corrente: |
21/11/2020 |
|
Data da última atualização: |
10/05/2021 |
|
Tipo da produção científica: |
Artigo em Periódico Indexado |
|
Circulação/Nível: |
B - 2 |
|
Autoria: |
BARBOSA NETO, M. V.; ARAÚJO, M. do S. B. de; ARAUJO FILHO, J. C. de; SAMPAIO, E. V. de S. B.; ALMEIDA, B. G. de. |
|
Afiliação: |
MANUELLA VIEIRA BARBOSA NETO, IFPE; MARIA DO SOCORRO BEZERRA DE ARAÚJO, UFPE; JOSE COELHO DE ARAUJO FILHO, CNPS; EVERARDO VALADARES DE SÁ BARRETTO SAMPAIO, UFPE; BRIVALDO GOMES DE ALMEIDA, UFRPE. |
|
Título: |
Rill and sheet soil erosion estimation in an area undergoing desertification in the Brazilian semi-arid region. |
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Ano de publicação: |
2021 |
|
Fonte/Imprenta: |
Modeling Earth Systems and Environment, v. 7, n. 2, p. 1183-1191, Jun. 2021. |
|
DOI: |
https://doi.org/10.1007/s40808-020-01026-y |
|
Idioma: |
Inglês |
|
Conteúdo: |
Soil erosion is a serious world problem, especially in areas undergoing desertification. Rill and sheet erosions were estimated in one municipality of the largest desertification nucleus in the Brazilian semi-arid region. Measurements were made in plots located in combinations of the two main soil classes (Luvisol and Planosol, 58 and 40% of the municipal area) and the two predominant vegetation covers (sparse and open, 84 and 7% of the municipal area). The sparse vegetation has 320 plants ha-1 covering 25% of the soil surface and the open vegetation has 495 plants ha-1, covering 40% of the soil surface. Length, width, and depth of all rills were measured in the plots to calculate the soil losses. Sheet erosion was estimated assuming that the height of the soil close to the bases of trees and shrubs in relation to the soil surface away from these bases corresponded to the depth of the lost soil layer. Rill erosion was higher under the sparse vegetation than under the open vegetation: 400 versus 45 Mg ha-1. Sheet erosion did not differ among soils and covers (547-860 Mg ha-1). Soil loss in the municipality was 34 Tg and 24 Eg when extrapolating to the desertification nucleus. Erosion and low vegetation cover are cumulative reinforcing degradation drivers, leading to low crop and livestock productivity, poverty, and social vulnerability. Land use restriction is the main measure to reduce erosion, but it increases social problems. |
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Palavras-Chave: |
Luvissolo. |
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Thesagro: |
Caatinga; Classificação do Solo; Cobertura Vegetal; Planossolo. |
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Thesaurus NAL: |
Luvisols; Planosols; Soil classification; Vegetation cover. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
|
Marc: |
LEADER 02380naa a2200289 a 4500
001 2126902
005 2021-05-10
008 2021 bl uuuu u00u1 u #d
024 7 $ahttps://doi.org/10.1007/s40808-020-01026-y$2DOI
100 1 $aBARBOSA NETO, M. V.
245 $aRill and sheet soil erosion estimation in an area undergoing desertification in the Brazilian semi-arid region.$h[electronic resource]
260 $c2021
520 $aSoil erosion is a serious world problem, especially in areas undergoing desertification. Rill and sheet erosions were estimated in one municipality of the largest desertification nucleus in the Brazilian semi-arid region. Measurements were made in plots located in combinations of the two main soil classes (Luvisol and Planosol, 58 and 40% of the municipal area) and the two predominant vegetation covers (sparse and open, 84 and 7% of the municipal area). The sparse vegetation has 320 plants ha-1 covering 25% of the soil surface and the open vegetation has 495 plants ha-1, covering 40% of the soil surface. Length, width, and depth of all rills were measured in the plots to calculate the soil losses. Sheet erosion was estimated assuming that the height of the soil close to the bases of trees and shrubs in relation to the soil surface away from these bases corresponded to the depth of the lost soil layer. Rill erosion was higher under the sparse vegetation than under the open vegetation: 400 versus 45 Mg ha-1. Sheet erosion did not differ among soils and covers (547-860 Mg ha-1). Soil loss in the municipality was 34 Tg and 24 Eg when extrapolating to the desertification nucleus. Erosion and low vegetation cover are cumulative reinforcing degradation drivers, leading to low crop and livestock productivity, poverty, and social vulnerability. Land use restriction is the main measure to reduce erosion, but it increases social problems.
650 $aLuvisols
650 $aPlanosols
650 $aSoil classification
650 $aVegetation cover
650 $aCaatinga
650 $aClassificação do Solo
650 $aCobertura Vegetal
650 $aPlanossolo
653 $aLuvissolo
700 1 $aARAÚJO, M. do S. B. de
700 1 $aARAUJO FILHO, J. C. de
700 1 $aSAMPAIO, E. V. de S. B.
700 1 $aALMEIDA, B. G. de
773 $tModeling Earth Systems and Environment$gv. 7, n. 2, p. 1183-1191, Jun. 2021.
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